Geochemistry and Os-Nd-Sr isotopes of the Gaositai Alaskan-type ultramafic complex from the northern North China craton: Implications for mantle-crust interaction

Contributions to Mineralogy and Petrology

Volumn 158, Issue 5, 2009, Pages 683-702

  Chen, Bin ^a,c   Suzuki, K ^b   Tian, W ^a,d   Jahn, B M ^c   Ireland, T ^d  

^a Peking University   (China)

^b JAPAN AGENCY FOR MARINE EARTH SCIENCE AND TECHNOLOGY   (Japan)

^c INSTITUTE OF EARTH SCIENCES   (Taiwan)

^d AUSTRALIAN NATIONAL UNIVERSITY   (Australia)

Author keywords

Alaskan type; North China craton; Os Nd Srisotopes; Ultramafic rocks

Indexed keywords

CLINOPYROXENE; CRUST-MANTLE BOUNDARY; CRUSTAL CONTAMINATION; ENRICHMENT; HORNBLENDE; IGNEOUS GEOCHEMISTRY; ISOTOPIC COMPOSITION; ISOTOPIC RATIO; MAGMATISM; MANTLE SOURCE; NEODYMIUM ISOTOPE; OSMIUM ISOTOPE; STRONTIUM ISOTOPE; SUBDUCTION ZONE; ULTRAMAFIC ROCK; ZONING;

ASIA; CHINA; EURASIA; FAR EAST; NORTH CHINA BLOCK;

EID: 70349224334     PISSN: 00107999     EISSN: None     Source Type: Journal    
DOI: 10.1007/s00410-009-0404-7     Document Type: Article

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